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Newspapers for this educational
program provided by:
NEWSPAPERS IN EDUCATION
This lesson is part of the Newspapers In Education program,
Oklahoma Rocks. To learn more visit nie.newsok.com.
A real life Jurassic Park existed in Oklahoma,
some 250–66 million years ago (mya),
during the Mesozoic Era. This time is known
as the “Age of the Dinosaurs.” Creatures
ranging from amphibians to dinosaurs roamed
Oklahoma, leaving fossils that tell us much of
their stories. Although there are fossils in the
southeast, northwest Oklahoma has proved
especially rich in dinosaur fossils. There is even
a dinosaur trackway preserved in the Morrison
Formation near Kenton, in Cimarron County. Due
to erosion, much of the evidence for dinosaurs in
other parts of the state is eroded away.
Oklahoma fossils of meat-eating dinosaurs from the Cretaceous Era (146–66 mya)
include Acrocanthosaurus atokensis and Deinonychus (southeast); and Jurassic
(200–146 mya) sauropods Apatosaurus (weighing 250 tons and 75 feet long, also known
as Brontosaurus), and Stegosaurus recovered from the Morrison Formation (northwest). The
giant Saurophaganax maximus fossils are unique to Oklahoma.
Fossils help: 1) Establish relative ages of marine and sedimentary rocks; 2) Reconstruct
depositional environments and climates; 3) Correlate rock strata around the world; and
4) Understand ancient plant and animal life and how climate change has affected the past.
Activities:
1. Using the geologic time scale http://ogs.ou.edu/level2-earthscied.php and internet,
think about what Oklahoma was like for dinosaurs. What was the climate like? How far
was it to the sea? What other life would they have seen?
2. Looking at the dinosaur footprint pictured with the 16-inch hammer, what might you
know about the dinosaur? How would you determine a dinosaur’s weight, size, and
how fast he/she was walking based on a trackway?
3. What might you learn about its habitat and when it lived from studying the rocks
around the footprint? See: http://ogs.ou.edu/level2-earthscied.php and an
Oklahoma trackway at: http://www.travelok.com/listings/view.profile/id.2245
Other tracks can be seen at the website for Dinosaur Ridge outside Denver: http://
www.dinoridge.org/discoveries.html or at Clayton Lake State Park just west of the OK
Panhandle: http://www.ucmp.berkeley.edu/mesozoic/cretaceous/clayton.html.
For more information on Oklahoma’s Acrocanthosaurus atokensis see:
http://www.museumoftheredriver.org/dino.html
For an activity on dinosaur names go to:
http://www.ucmp.berkeley.edu/fosrec/MunGun4.html
Dinosaur track near Kenton, Oklahoma,
shows three toes. The hammer to the left of
the track is 16 inches long.

Newspapers for this educational
program provided by:
NEWSPAPERS IN EDUCATION
This lesson is part of the Newspapers In Education program,
Oklahoma Rocks. To learn more visit nie.newsok.com.
A real life Jurassic Park existed in Oklahoma,
some 250–66 million years ago (mya),
during the Mesozoic Era. This time is known
as the “Age of the Dinosaurs.” Creatures
ranging from amphibians to dinosaurs roamed
Oklahoma, leaving fossils that tell us much of
their stories. Although there are fossils in the
southeast, northwest Oklahoma has proved
especially rich in dinosaur fossils. There is even
a dinosaur trackway preserved in the Morrison
Formation near Kenton, in Cimarron County. Due
to erosion, much of the evidence for dinosaurs in
other parts of the state is eroded away.
Oklahoma fossils of meat-eating dinosaurs from the Cretaceous Era (146–66 mya)
include Acrocanthosaurus atokensis and Deinonychus (southeast); and Jurassic
(200–146 mya) sauropods Apatosaurus (weighing 250 tons and 75 feet long, also known
as Brontosaurus), and Stegosaurus recovered from the Morrison Formation (northwest). The
giant Saurophaganax maximus fossils are unique to Oklahoma.
Fossils help: 1) Establish relative ages of marine and sedimentary rocks; 2) Reconstruct
depositional environments and climates; 3) Correlate rock strata around the world; and
4) Understand ancient plant and animal life and how climate change has affected the past.
Activities:
1. Using the geologic time scale http://ogs.ou.edu/level2-earthscied.php and internet,
think about what Oklahoma was like for dinosaurs. What was the climate like? How far
was it to the sea? What other life would they have seen?
2. Looking at the dinosaur footprint pictured with the 16-inch hammer, what might you
know about the dinosaur? How would you determine a dinosaur’s weight, size, and
how fast he/she was walking based on a trackway?
3. What might you learn about its habitat and when it lived from studying the rocks
around the footprint? See: http://ogs.ou.edu/level2-earthscied.php and an
Oklahoma trackway at: http://www.travelok.com/listings/view.profile/id.2245
Other tracks can be seen at the website for Dinosaur Ridge outside Denver: http://
www.dinoridge.org/discoveries.html or at Clayton Lake State Park just west of the OK
Panhandle: http://www.ucmp.berkeley.edu/mesozoic/cretaceous/clayton.html.
For more information on Oklahoma’s Acrocanthosaurus atokensis see:
http://www.museumoftheredriver.org/dino.html
For an activity on dinosaur names go to:
http://www.ucmp.berkeley.edu/fosrec/MunGun4.html
Dinosaur track near Kenton, Oklahoma,
shows three toes. The hammer to the left of
the track is 16 inches long.